Plant and soil nitrogen in oligotrophic boreal forest habitats with varying moss depths:does exclusion of large grazers matter?

The boreal forest consists of drier sunlit and moister-shaded habitats with varying moss abundance. Mosses control vascular plant–soil interactions, yet they all can also be altered by grazers. We determined how 2 decades of reindeer (Rangifer tarandus) exclusion affect feather moss (Pleurozium schr...

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Bibliographic Details
Published in:Oecologia
Main Authors: Väisänen, Maria, Tuomi, Maria, Bailey, Hannah, Welker, Jeffrey M.
Format: Article in Journal/Newspaper
Language:English
Published: 2021
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Online Access:https://research.ulapland.fi/fi/publications/7cee46a2-a21b-4ed6-a93e-1c5f81f8c3d3
https://doi.org/10.1007/s00442-021-04957-0
https://lacris.ulapland.fi/ws/files/16836864/Va_isa_nen_et_al._2021.docx
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Summary:The boreal forest consists of drier sunlit and moister-shaded habitats with varying moss abundance. Mosses control vascular plant–soil interactions, yet they all can also be altered by grazers. We determined how 2 decades of reindeer (Rangifer tarandus) exclusion affect feather moss (Pleurozium schreberi) depth, and the accompanying soil N dynamics (total and dissolvable inorganic N, δ 15 N), plant foliar N, and stable isotopes (δ 15 N, δ 13 C) in two contrasting habitats of an oligotrophic Scots pine forest. The study species were pine seedling (Pinus sylvestris L.), bilberry (Vaccinium myrtillus L.), lingonberry (V. vitis-idaea L.), and feather moss. Moss carpet was deeper in shaded than sunlit habitats and increased with grazer exclusion. Humus N content increased in the shade as did humus δ 15 N, which also increased due to exclusion in the sunlit habitats. Exclusion increased inorganic N concentration in the mineral soil. These soil responses were correlated with moss depth. Foliar chemistry varied due to habitat depending on species identity. Pine seedlings showed higher foliar N content and lower foliar δ 15 N in the shaded than in the sunlit habitats, while bilberry had both higher foliar N and δ 15 N in the shade. Thus, foliar δ 15 N values of co-existing species diverged in the shade indicating enhanced N partitioning. We conclude that despite strong grazing-induced shifts in mosses and subtler shifts in soil N, the N dynamics of vascular vegetation remain unchanged. These indicate that plant–soil interactions are resistant to shifts in grazing intensity, a pattern that appears to be common across boreal oligotrophic forests.